modeling group dispersal of particles with a
play

Modeling group dispersal of particles with a spatiotemporal point - PowerPoint PPT Presentation

Modeling group dispersal of particles with a spatiotemporal point process Samuel Soubeyrand INRA Biostatistics and Spatial Processes Joint work with L. Roques, J. Coville and J. Fayard 9th SSIAB Workshop, May 10, 2012 Group Dispersal


  1. Modeling group dispersal of particles with a spatiotemporal point process Samuel Soubeyrand INRA – Biostatistics and Spatial Processes Joint work with L. Roques, J. Coville and J. Fayard 9th SSIAB Workshop, May 10, 2012 Group Dispersal Project – Plant Health and Environment Dpt.

  2. Spatiotemporal point processes in propagation models Object of interest: species spreading using small particles (spores, pollens, seeds...) Sources of particles generate a spatially structured rain of particles ◮ rain of particles → spatial point process ◮ spatial structure → inhomogeneous intensity of the process

  3. Intensity of the spatial point process formed by the deposit locations of the particles The intensity is a convolution between ◮ the source process (spatial pattern and strengths) and ◮ a parametric dispersal kernel

  4. Simulation of an epidemics

  5. Dispersal kernel Dispersal kernel: probability density function of the deposit location of a particle released at the origin The shape of the kernel is a major topic in dispersal studies: it determines ◮ the propagation speed ◮ the spatial structure of the population ◮ the genetic structure of the population

  6. Main characteristics of dispersal kernels: ◮ long distance dispersal (Minogue, 1989) ◮ non-monotonicity (Stoyan and Wagner, 2001) 200 Intensity 0.5 ◮ anisotropy 0.1 100 0.01 0.001 Ordinate (m) 0 − 100 − 200 − 300 − 200 − 100 0 50 100 Abscissa (m)

  7. Observation of secondary foci (clusters) in real epidemics Epidemics of yellow rust of wheat in an experimental field (I. Sache) t = 1 t = 2 t = 3 t = 4

  8. ◮ Classical justifications for patterns with multiple foci: ◮ long distance dispersal ◮ spatial heterogeneity ◮ super-spreaders (a few individuals which infects many susceptible individuals)

  9. ◮ Classical justifications for patterns with multiple foci: ◮ long distance dispersal ◮ spatial heterogeneity ◮ super-spreaders (a few individuals which infects many susceptible individuals) ◮ An other justification to be investigated: Group dispersal ◮ Groups of particles are released due to wind gusts ◮ Particles of any group are transported in an expanding air volume ◮ At a given stopping time, particles of any group are projected to the ground

  10. Group Dispersal Model (GDM): Spatial case Deposit equation for particles: A single point source of particles located at the origin of R 2 J : number of groups of particles released by the source N j : number of particles in group j ∈ { 1 , . . . , J } X jn : deposit location of the n th particle of group j satisfying X jn = X j + B jn ( ν || X j || ) , (1) where X j : final location of the center of group j , B jn : Brownian motion describing the relative movement of the n th particle in group j with respect to the group center ν : positive parameter

  11. Assumptions about the deposit equation ◮ The random variables J , N j , X j and the random processes { B jn : n = 1 , . . . , N j } are mutually independent ◮ Number of groups: J ∼ Poisson ( λ ) ◮ Number of particles in group j : N j ∼ indep p µ, σ 2 ( · ) ◮ Group center location: X j ∼ indep f X j ( · ) (features of f X j : decrease at the origin is more or less steep, tail more or less heavy, shape more or less anisotropic...) ◮ The Brownian motions B jn are centered, independent and with independent components They are stopped at time t = ν || X j || . Then, B jn ( ν || X j || ) ∼ indep N (0 , ν || X j || I )

  12. Dispersal from a single source ◮ Simulations: (Interpretation: Cox process or Neyman-Scott with double nonstationarity — in the center pattern and the o ff spring di ff usion) Ordinate D e n Ordinate s i t y Abscissa Abscissa 0.3 0.2 0.1 Ordinate 0.0 − 0.1 I n t Ordinate e n s i t y − 0.2 − 0.3 Abscissa − 0.3 − 0.2 − 0.1 0.0 0.1 0.2 0.3 0.4 Abscissa Marginal probability density function (dispersal kernel):

  13. Dispersal from a single source ◮ Simulations: (Interpretation: Cox process or Neyman-Scott with double nonstationarity — in the center pattern and the o ff spring di ff usion) Ordinate D e n Ordinate s i t y Abscissa Abscissa ◮ Marginal probability density function (dispersal kernel): � � f X jn ( x ) = R 2 f X jn | X j ( x | y ) f X j ( y ) dy = R 2 φ ν , y ( x ) f X j ( y ) dy . The particles are n.i.i.d. from this p.d.f. while in the classical dispersal models the particles are i.i.d. from a dispersal kernel which may be of the form of f X j or f X jn

  14. Discrepancies from independent dispersal The GDM is compared with two independent dispersal models (IDM) ◮ IDM1: the number of particles in each group is assumed to be one. Thus, particles are independently drawn under the p.d.f. f X jn . ◮ IDM2: the number of particles in each group is assumed to be one and the Brownian motions are deleted (i.e. ν = 0). Thus, particles are independently drawn under the p.d.f. f X j .

  15. Moments X : Deposit location of a particle Q ( x + dx ): Count of points in x + dx Criterion Model Value ( 0 E ( X ) GDM 0 ) ( 0 IDM1 0 ) ( 0 IDM2 0 ) V ( X ) GDM V ( X j ) + ν E ( || X j || ) I IDM1 V ( X j ) + ν E ( || X j || ) I IDM2 V ( X j ) E ( || X || 2 ) E ( || X j || 2 ) + 2 ν E ( || X j || ) GDM E ( || X j || 2 ) + 2 ν E ( || X j || ) IDM1 E ( || X j || 2 ) IDM2 E { Q ( x + dx ) } GDM λ µ f X jn ( x ) dx IDM1 λ f X jn ( x ) dx IDM2 λ f X j ( x ) dx λ [ µ f X jn ( x ) dx + ( σ 2 + µ 2 − µ ) E { φ ν , X j ( x ) 2 } ( dx ) 2 ] V { Q ( x + dx ) } GDM IDM1 λ f X jn ( x ) dx IDM2 λ f X j ( x ) dx λ ( σ 2 + µ 2 − µ ) E { φ ν , X j ( x 1 ) φ ν , X j ( x 2 ) } ( dx ) 2 cov { Q ( x 1 + dx ) GDM , Q ( x 2 + dx ) } IDM1 0 IDM2 0

  16. GDM: larger variance of Q ( x + dx ) and positive covariance (decreasing with distance) → clusters (even with µ = 1) We expect multiple foci in the spatio-temporel case

  17. Group dispersal model: Spatio-temporal case → multiple foci under the GDM Ordinate Ordinate − 1.0 − 0.5 0.0 0.5 1.0 − 1.0 − 0.5 0.0 0.5 1.0 GDM − 1.0 − 1.0 − 0.5 − 0.5 0.0 Abscissa Abscissa 0.0 0.5 0.5 1.0 1.0 0 10000 20000 30000 40000 50000 60000 Ordinate Ordinate − 1.0 − 0.5 0.0 0.5 1.0 − 1.0 − 0.5 0.0 0.5 1.0 − 1.0 IDM1 − 1.0 − 0.5 − 0.5 0.0 Abscissa Abscissa 0.0 0.5 0.5 1.0 1.0 0 10000 20000 30000 40000 Ordinate Ordinate − 1.0 − 0.5 0.0 0.5 1.0 − 1.0 − 0.5 0.0 0.5 1.0 − 1.0 − 1.0 IDM2 − 0.5 − 0.5 0.0 Abscissa Abscissa 0.0 0.5 0.5 1.0 1.0 0 5000 10000 15000 20000 25000

  18. Simulation study of the number of foci: Definition A δ -focus is a set of cells (from a regular grid) which are connected and whose intensity of points is larger than δ model ν 2 model ν 2 σ σ 8 8 IDM2 0 0 GDM 0.001 50 IDM1 0.005 0 GDM 0.005 50 GDM 0.005 10 GDM 0.01 50 GDM 0.005 50 GDM 0.1 50 6 6 Number of − foci Number of − foci GDM 0.005 100 δ δ 4 4 2 2 0 0 0 50000 100000 150000 0 50000 100000 150000 Threshold δ Threshold δ

  19. Farthest particle (link with propagation speed) Definition The maximum dispersal distance during one generation is R max = max { R jn : j ∈ J , n ∈ N j } where R jn = || X jn || J = { 1 , . . . , J } if J > 0 and the empty set otherwise N j = { 1 , . . . , N j } if N j > 0 and the empty set otherwise By convention, if no particle is released ( J = 0 or N j = 0 for all j ), then R max = 0 Ordinate Abscissa

  20. R max = max { R jn : j ∈ J , n ∈ N j } Under the GDM and IDMs, the distribution of the distance between the origin and the furthest deposited propagule is zero-inflated and satisfies: P ( R max = 0) = exp � � λ { p µ, σ 2 (0) − 1 } f R max ( r ) = λ f R max ( r ) exp { λ ( F R max ( r ) − 1) } , ∀ r > 0 , j j is the p.d.f. of the distance R max where f R max = max { R jn : n ∈ N j } j j between the origin and the furthest deposited propagule of group j , and F R max is the corresponding cumulative distribution function j � r ( r ) = P ( R max ( F R max = 0) + 0 f R max ( u ) du ). j j j → Distribution of R max ? j

  21. Under the IDMs, N j = 1 for all j ∈ J and, consequently, p µ, σ 2 (0) = 0 and f R max ( r ) = f R jn ( r ) j �� 2 π rf X jn (( r cos θ , r sin θ )) d θ for the IDM1 0 = � 2 π rf X j (( r cos θ , r sin θ )) d θ for the IDM2 . 0

  22. Under the GDM, the distribution of R max is zero-inflated and j satisfies: P ( R max = 0) = p µ, σ 2 (0) j � f R max ( r ) = R 2 f R max | X j ( r | x ) f X j ( x ) dx j j + ∞ � � R 2 f R jn | X j ( r | x ) F R jn | X j ( r | x ) q − 1 f X j ( x ) dx , = qp µ, σ 2 ( q ) q =1 where f R jn | X j is the conditional distribution of R jn given X j satisfying � r 2 h 1 ( u , x ) h 2 ( r 2 − u , x ) du , f R jn | X j ( r | x ) = 2 r 0 h i ( u , x ) = f i ( √ u , x ) + f i ( −√ u , x ) ∀ i ∈ { 1 , 2 } , 2 √ u , � � − ( v − x ( i ) ) 2 1 f i ( v , x ) = exp ∀ i ∈ { 1 , 2 } , , � 2 ν || x || 2 πν || x || � r x = ( x (1) , x (2) ) and F R jn | X j ( r | x ) = 0 f R jn | X j ( s | x ) ds .

Download Presentation
Download Policy: The content available on the website is offered to you 'AS IS' for your personal information and use only. It cannot be commercialized, licensed, or distributed on other websites without prior consent from the author. To download a presentation, simply click this link. If you encounter any difficulties during the download process, it's possible that the publisher has removed the file from their server.

Recommend


More recommend